马超营一一潘河大断裂,界定了古生代时期华北板块活动大陆边缘陆架与陆缘表海的南部边沿。
The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.
马超营一一潘河大断裂,界定了古生代时期华北板块活动大陆边缘陆架与陆缘表海的南部边沿。
The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.
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